1) coastal plain of south Hangzhou bay bank
杭州湾南岸滨海平原
1.
The paper analyzed the land use change on the coastal plain of south Hangzhou bay bank.
文章以土地利用动态数据为基础,应用生态学、生态经济学等方法分析了杭州湾南岸滨海平原土地利用变化所引起的生态系统服务价值变化。
2) south coast of Hangzhou bay
杭州湾南岸
1.
Granularity analyses of superficial sediments of Sparitina alterniflora flat on south coast of Hangzhou Bay;
杭州湾南岸互花米草潮滩底质粒度及其分布特征
2.
<Abstrcat>Based on the Universal Soil Loss Equation (USLE), the authors analyse the function for soil conservation of agro-ecosystems and its eco-economic value in south coast of Hangzhou bay.
文章运用土壤通用流失方程(USLE)研究了杭州湾南岸农业生态系统的土壤保持功能,并评价了其经济价值。
3) south coast of Hangzhouwan bay
杭州湾南岸
1.
The paper discussed the granularity of superficial sediments of Spartina alterniflora salt marsh on the south coast of Hangzhouwan bay.
分析杭州湾南岸互花米草滩内外表层沉积物的粒度特征,互花米草生物海岸沉积物包括粘土质粉砂、粉砂、粉砂质砂和砂质粉砂4类,由东向西各断面草滩内、外沉积物中值粒径逐渐变粗,分选性变好;从低潮滩向高潮滩沉积物的中值粒径Φ值增大,分选性变差。
2.
Based on analysis of the natural and soc-economic characters of south coast of Hangzhouwan bay and results of Costanza et al,the methods of ecological economics and ecology were applied to analyze the economic values on the south coast of Hangzhouwan bay.
该文应用生态学、生态经济学方法及Costanza等的研究成果,结合杭州湾南岸生态系统的自然和社会经济特征的分析,初步估算出2000年杭州湾南岸生态系统服务功能的总价值为91 1亿元,其中间接经济价值是直接经济价值的5 85倍,并对各种生态系统类型的服务价值构成进行了讨论。
4) south coast plain of Laizhou Bay
莱州湾南岸平原
1.
According to the chemical analyses data of the groundwater samples from 129 hydrogeologic drill-holes,and the groundwater mineralization degree data of 1200 wells tested in the field,the hydrochemical environments of the groundwater in the south coast plain of Laizhou Bay,especially the hydrochemical environments of the shallow groundwater in the salt water intrusion area,have been studied.
根据129个水文地质钻孔及其地下水水样的水质分析结果和1200眼井的地下水矿化度野外实测资料,研究了莱州湾南岸平原的地下水水化学环境,尤其是咸水入侵区的浅层地下水水化学环境特
2.
By field investigation and water chemical monitoring, the groundwater environment of the shallow buried paleochannel zones and alluvial diluvial fans on the south coast plain of Laizhou Bay can be divided into 3 area: the salt groundwater district in the north, the transition district in the middle and the fresh groundwater district in the south.
通过野外实地调查和水化学监测,将莱州湾南岸平原浅埋古河道带及冲洪积扇浅层地下水水化学环境分为3大区域,即北部的全咸水区、中部的咸淡水过渡区和南部的全淡水区。
5) the north of Hangzhou Bay
杭州湾北岸
1.
Based on the data extracted from bathymetric maps and data obtained through hydrological and sediment surveys,this paper mainly deals with the evolution of siltation and erosion of the Jinhui tidal flat in the north of Hangzhou Bay.
杭州湾北岸在南汇嘴和金山嘴人工控制节点作用下,形成微弯内凹的弧形海岸廓线,金汇岸段位于弧形岸线凹段。
6) across the Hangzhou Bay
杭州湾两岸
1.
Culture and Environment across the Hangzhou Bay in the Neolithic Age;
杭州湾两岸新石器时代文化与环境
补充资料:杭州湾
杭州湾 位于中国浙江省东北部。有钱塘江注入,是一个喇叭形海湾。湾口宽约95千米,海宁一带仅宽3千米。自乍浦至仑前,七堡至闻家堰一带水下形成巨大的沙坎(洲),长130千米,宽约27千米,厚约20米。北侧金山卫一乍浦之间的沿岸海底有一巨大的冲刷槽,最深约40米。湾底的地貌形态和海湾的喇叭形特征,使这里常出现涌潮或暴涨潮。杭州湾以海宁潮(钱塘潮)著称,是中国沿海潮差最大的海湾,历史上最大潮差曾达8.93米。湾外为舟山群岛。 |
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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